Harney Basin

Coordinates: 43°30′N 119°00′W / 43.5°N 119°W / 43.5; -119
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The Harney Basin

The Harney Basin is an arid basin (and a physiographic section) in southeastern Oregon in the United States, at the northwestern corner of the Great Basin. One of the least populated areas of the contiguous United States, it is located largely in northern Harney County, bounded on the north and east by the Columbia Plateau (of which it is contained within, physiographically) and the south and west by a volcanic plain. The basin encompasses an area of 5,300 square miles (13,727 km2)[1] in the watershed of Malheur Lake and Harney Lake. Malheur Lake is a freshwater lake, while Harney Lake is saline-alkaline.[2]

Description

The basin is specifically bounded on the north by the southern end of the Blue Mountains. The ridge of Steens Mountain separates the basin from the watershed of the Alvord Desert to the southeast.[3] No streams cross the volcanic plains that separate the basin from the watershed of the Klamath River to the southwest.

The central basin receives an average of 6 in (150 mm) of rain per year, with the surrounding mountains receiving an average of 15 in (380 mm) per year. The center of the basin is a flat lowlands containing Malheur and Harney lakes, which receive the streams within the basin from the surrounding mountains, including the Silvies River from the north and the Donner und Blitzen River from the south. Harney Lake is the actual sink of the basin, connected in some years to Malheur Lake but currently separated by constantly changing sand dunes. Both lakes cycle between open water in wetter years and marshes in drier years.

The wetlands around Malheur Lake and Harney Lake form a wetlands oasis in the basin, providing a habitat for many migratory bird species, including 2.5 million ducks each year. Malheur Lake and its surroundings are embraced by Malheur National Wildlife Refuge.

The basin has a total population of fewer than 10,000 people. The only community with a population larger than 1,000 is Burns which sits in the plain north of Malheur Lake. Dryland ranching is the basis of economy, with little relatively irrigation water available from the streams that enter Malheur Lake.

History

The basin was formed approximately 32,000 years ago when lava flows formed the Malheur Gap, separating the watershed of the basin from the Malheur River, a tributary of the Snake River. Archaeological evidence indicates the basin was inhabited as early as 10,000 years ago. Pollen records indicate that the climate, especially the level of rain and snowfall, has varied greatly since the end of the Pleistocene. Evidence of prehistoric fishing techniques is found at several sites. Evidence suggests that several species--in particular the chiselmouth, coarse-scale suckers, and northern squawfish--existed in the basin that are currently found only in the Columbia River basin; indicating that at some point the basin may have been connected to the Columbia. During wetter years, the lake level of Malheur Lake was raised to a depth of 25 ft (7.5 m), allowing the lakes to drain over the Malheur Gap. In modern times, however, the lake level does not rise above 10 ft (3 m) in the wettest years.

In the 19th century the basin was inhabited by the Northern Paiute tribe. It was explored and extensively trapped by trappers of the Hudson's Bay Company in the 1820s. The basin lay far off the route of the Oregon Trail, but in 1843 experienced mountain man Stephen Meek led an ill-fated party across the basin via Stinkingwater Pass, seeking a shortcut to The Dalles along what has become known as the Meek Cutoff. A total of 23 people died while the party wandered in the basin until finding water at the Crooked River.

Because of its climate it received little white settlement and was largely left to the Paiute until the late 19th century. Settlement pressures and conflicts with the Paiute in other ares of Oregon caused President Ulysses S. Grant in 1872 to create a reservation for the Paiute encompassing Malheur Lake and much of the basin. Growing settlement pressures, in particular the discovery of gold in the surrounding mountains, as well as the interest of white settlers to form ranches in the region, caused Grant to abruptly terminate the reservation in 1879. The Northern Paiute would survive virtually landless until obtaining tracts of land near Burns in 1935.

See also

References

  1. ^ {{citation}}: Empty citation (help)
  2. ^ GREATER HARNEY BASIN AGRICULTURAL WATER QUALITY MANAGEMENT AREA PLAN, p. 15 & p. 17ff (.PDF)
  3. ^ Google Earth: bbs.keyhole.com/ubb/placemarks/cl-03-20-06-980475833.kmz

External links

43°30′N 119°00′W / 43.5°N 119°W / 43.5; -119

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